Methods and apparatus for
atmospheric sounding using acoustic chirps are disclosed, the transmitted and echo chirps being compared in a mixer that yields frequency sums and differences. Preferably, the mixing is performed as a complex multiplication in the
Fourier domain. In one
system (1) a
signal generator (5) such as a PC
sound card drives a
loudspeaker (3) that serves as a
transmitter and echo pulses are detedcted by a
microphone (4) that serves as a
receiver. Chirps transmitted by the
loudspeaker (3) travel by different paths (7a and 7b) due to reflection from TILS or thermal inversion
layers (2a and 2b) at different altitudes. The transmitted and echo
chirp signals are compared in a mixer (6) from which various outputs (8 and 9) can be generated. One output (8) might be the magnitude of the difference between the transmitted and echo
chirp tones, instant by instant, which is indicative of the altitudes of the respective TILs. The other output (9) might be the phase shift in an echo tone with
transit time, which is indicative of vertical wind velocity at different altitudes. Such sounding methods and apparatus are useful for weather research, prediction of plume dispersal and the design of
microwave links to minimize multipath
fading.